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19 results were found for Tải Google Screen(TG:e10838).lth.


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  • 11. A new absolute minimum temperature record

    station at Grímsstaðir is new, however, established last autumn only. There, measurements at the old manual station are still ongoing. The in-screen minimum thermometer registered “only” -14.5°C on the morning of 2 May. The distance between the two stations is less than 100 meters. The registrations at the new automatic station at Grímsstaðir have not been compared to the manual registration /about-imo/news/nr/2691
  • 12. The weather in Iceland 2010

    was unusually light. The barometric pressure reached the highest annual value on record. The climate was very favourable and windstorms markedly fewer than usual. Temperature Thermometer screen at IMO's grounds in Reykjavík. Photo by Jón Gunnar Egilsson, 15 September 2010. Temperature The average temperature in Reykjavík was 5.9°C, 1.6°C above the 1961 to 1990 mean, and has only once /about-imo/news/2011/nr/2112
  • 13. The weather in Iceland 2010

    was unusually light. The barometric pressure reached the highest annual value on record. The climate was very favourable and windstorms markedly fewer than usual. Temperature Thermometer screen at IMO's grounds in Reykjavík. Photo by Jón Gunnar Egilsson, 15 September 2010. Temperature The average temperature in Reykjavík was 5.9°C, 1.6°C above the 1961 to 1990 mean, and has only once /about-imo/news/nr/2112
  • 14. ved-eng-2010

    of the country where the year was one of the warmest and driest on record and the snowfall was unusually light. The barometric pressure reached the highest annual value on record. The climate was very favorable and windstorms markedly fewer than usual. Temperature Thermometer screen at IMO's grounds in Reykjavík. Photo by Jón Gunnar Egilsson, 15 September 2010. Temperature /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf
  • 15. IPPC-2007-ar4_syr

  • 16. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  • 17. VI_2021_008

    a coherent, emergent signal in RSAM data (see Figure 2), raising the question: Can RSAM data be empirically used to detect volcanic tremor events preceding eruptions? 6 Figure 1. Photo of the monitoring setup in the IMO’s natural hazards monitoring room. The right screen shows real-time earthquake and tremor data. Tremv output is displayed in red box with the last 24 hrs of all frequency /media/vedurstofan-utgafa-2021/VI_2021_008.pdf
  • 18. vonKorff_etal-2010

    They are either widely cited, e.g., Stern and Fineberg (1996) and Beierle and Cayford (2002) in Google Scholar; widely used in higher education, e.g., Creighton (2005); or are French-language guides, e.g., d’Aquino (2008) and Mazri (2007). Because of our own work background in French-speaking countries, we particularly wanted to include the latter to add useful diversity to our study. Because citation /media/loftslag/vonKorff_etal-2010.pdf
  • 19. vanRoosmalen_etal-2009-WRR_2007WR006760

    in Figure 2). The well screen is located 5.65 m below ground surface at location A and 25.5 m below ground surface at location B. Generally the model captures the dynamics in the time series well, even though the mean simulated and observed values may differ considerably. Therefore this study focuses on spatially averaged changes when comparing one simu- lation to the other and less on the absolute /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

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